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• 31. [Article] Trout studies and a stream survey of Crater Lake National Park, Oregon

  Citation × Citation Citation Abstract Copy Title: Trout studies and a stream survey of Crater Lake National Park, Oregon Author: Wallis, O. L. Title: Trout studies and a stream survey of Crater Lake National Park, Oregon Author: Wallis, O. L. Close

• 32. [Article] A survey of the waters of the South Umpqua Ranger District : Umpqua National Forest

  Citation × Citation Citation Abstract Copy Title: A survey of the waters of the South Umpqua Ranger District : Umpqua National Forest Author: Roth, A. R. Title: A survey of the waters of the South Umpqua Ranger District : Umpqua National Forest Author: Roth, A. R. Close

• 33. [Article] A suggested outline and procedure for making a sanitary stream survey with particular reference to Mary's River of Oregon

  Citation × Citation Citation Abstract Copy Title: A suggested outline and procedure for making a sanitary stream survey with particular reference to Mary's River of Oregon Author: Morgan, William D. Title: A suggested outline and procedure for making a sanitary stream survey with particular reference to Mary's River of Oregon Author: Morgan, William D. Close

• 34. [Article] Ocean data assimilation using optimal interpolation with a quasi-geostrophic model

  Copyrighted by American Geophysical Union.

  Citation × Citation Citation Abstract Copy Title: Ocean data assimilation using optimal interpolation with a quasi-geostrophic model Author: Miller, Robert N., Rienecker, Michele M. Copyrighted by American Geophysical Union. Title: Ocean data assimilation using optimal interpolation with a quasi-geostrophic model Author: Miller, Robert N., Rienecker, Michele M. Copyrighted by American Geophysical Union. Close

• 35. [Article] Response of western Oregon stream temperatures to contemporary forest management

  This is the author's peer-reviewed final draft as accepted by the publisher. The final version is copyrighted by Elsevier and can be found at the Forest Ecology and Management website: http://www.elsev...

  Citation × Citation Citation Abstract Copy Title: Response of western Oregon stream temperatures to contemporary forest management Author: Madsen, Lisa J., Dent, Liz, Groom, Jeremiah D., Fleuret, Jennifer This is the author's peer-reviewed final draft as accepted by the publisher. The final version is copyrighted by Elsevier and can be found at the Forest Ecology and Management website: http://www.elsevier.com/wps/find/journaldescription.cws_home/503310/description Title: Response of western Oregon stream temperatures to contemporary forest management Author: Madsen, Lisa J., Dent, Liz, Groom, Jeremiah D., Fleuret, Jennifer This is the author's peer-reviewed final draft as accepted by the publisher. The final version is copyrighted by Elsevier and can be found at the Forest Ecology and Management website: http://www.elsevier.com/wps/find/journaldescription.cws_home/503310/description Close

• 36. [Article] Effects of beaver on streams, streamside habitat, and coho salmon fry populations in two coastal Oregon streams

  The effects of beaver (Castor canadensis) on stream morphology, riparian zones, and coho salmon (Oncorhynchus kisutch) fry in Cape and Cummins Creeks, Oregon, were examined using stream surveys, vegetation ...

  Citation × Citation Citation Abstract Copy Title: Effects of beaver on streams, streamside habitat, and coho salmon fry populations in two coastal Oregon streams Author: Bruner, Karen L. The effects of beaver (Castor canadensis) on stream morphology, riparian zones, and coho salmon (Oncorhynchus kisutch) fry in Cape and Cummins Creeks, Oregon, were examined using stream surveys, vegetation transects, and coho salmon fry counts in 1987. The basin around Cape Creek has been extensively logged since the late 1940's. Cummins Creek is surrounded by primarily old-growth forest. Cape Creek had higher densities of coho fry (P < 0.0004) than Cummins Creek. Coho fry were two to ten times more numerous in pools (P < 0.001) than in glides or riffles, respectively. The density of beaver dams in the autumn on the two streams was 1.2 and 1.1 dams/km on Cummins and Cape Creeks, respectively. By building dams, beaver added 7% and 14% more pool habitat in Cummins and Cape Creeks, respectively. This extra pool habitat was used by coho fry. Beaver ponds were larger than non-beaver ponds and thus contained more coho fry per pond. Densities of coho fry were, however, the same between beaver and non-beaver ponds. Beaver preferred to cut salmonberry (Rubus spectabilis), alder (Alnus rubra), and vine maple (Acer circinatum) stems 2-9 cm in diameter for food and dam construction. Mean distance from the stream for foraging was 17.5 m (SDS=10.1). Beaver foraged up to 90 in from the stream bank along tributaries. The percentage of available stems (for salmonberry, alder, and vine maple) cut for the small size class (0.5-3 cm) decreased after 5 in from the stream, after 20 in for the medium size class (3-9 cm) and remained stable out to 30 m for the large size class ( > 9 cm). Most cutting tended to be upstream of the dam site. The mean area affected by cutting around the dam site was 1944 sq. in (SD=921 sq. m). Proximity to a logjam, tributary, or debris slide; midstory conifer cover; overstory conifer cover; and vine maple cover were factors that separated used beaver sites from unused random sites using stepwise discriminant analysis. Proximity to a logjam, tributary, or debris slide was positively associated with the discriminant function and accounted for 50% of the variability in the discriminant function. Vine maple cover was also positively associated with dam location in the discriminant function, while midstory and overstory conifer covers were negatively associated with the dam location. Based on the results of this study, I believe beaver provide extra coho salmon rearing habitat, especially in late summer during reduced water flows. In heavily managed streams, beaver may be able to provide structure and stability in the stream at a much lower cost than stream rehabilitation projects. Title: Effects of beaver on streams, streamside habitat, and coho salmon fry populations in two coastal Oregon streams Author: Bruner, Karen L. The effects of beaver (Castor canadensis) on stream morphology, riparian zones, and coho salmon (Oncorhynchus kisutch) fry in Cape and Cummins Creeks, Oregon, were examined using stream surveys, vegetation transects, and coho salmon fry counts in 1987. The basin around Cape Creek has been extensively logged since the late 1940's. Cummins Creek is surrounded by primarily old-growth forest. Cape Creek had higher densities of coho fry (P < 0.0004) than Cummins Creek. Coho fry were two to ten times more numerous in pools (P < 0.001) than in glides or riffles, respectively. The density of beaver dams in the autumn on the two streams was 1.2 and 1.1 dams/km on Cummins and Cape Creeks, respectively. By building dams, beaver added 7% and 14% more pool habitat in Cummins and Cape Creeks, respectively. This extra pool habitat was used by coho fry. Beaver ponds were larger than non-beaver ponds and thus contained more coho fry per pond. Densities of coho fry were, however, the same between beaver and non-beaver ponds. Beaver preferred to cut salmonberry (Rubus spectabilis), alder (Alnus rubra), and vine maple (Acer circinatum) stems 2-9 cm in diameter for food and dam construction. Mean distance from the stream for foraging was 17.5 m (SDS=10.1). Beaver foraged up to 90 in from the stream bank along tributaries. The percentage of available stems (for salmonberry, alder, and vine maple) cut for the small size class (0.5-3 cm) decreased after 5 in from the stream, after 20 in for the medium size class (3-9 cm) and remained stable out to 30 m for the large size class ( > 9 cm). Most cutting tended to be upstream of the dam site. The mean area affected by cutting around the dam site was 1944 sq. in (SD=921 sq. m). Proximity to a logjam, tributary, or debris slide; midstory conifer cover; overstory conifer cover; and vine maple cover were factors that separated used beaver sites from unused random sites using stepwise discriminant analysis. Proximity to a logjam, tributary, or debris slide was positively associated with the discriminant function and accounted for 50% of the variability in the discriminant function. Vine maple cover was also positively associated with dam location in the discriminant function, while midstory and overstory conifer covers were negatively associated with the dam location. Based on the results of this study, I believe beaver provide extra coho salmon rearing habitat, especially in late summer during reduced water flows. In heavily managed streams, beaver may be able to provide structure and stability in the stream at a much lower cost than stream rehabilitation projects. Close

• 37. [Article] A physical inventory of streams in the Upper Willamette Watershed above the confluence of middle and coast forks of Willamette River : 1964

  Dimensions of paper map: 37" x 37.5".

  Citation × Citation Citation Abstract Copy Title: A physical inventory of streams in the Upper Willamette Watershed above the confluence of middle and coast forks of Willamette River : 1964 Author: Oregon. State Game Commission. Basin Investigations Section, Thompson, Kenneth E. Dimensions of paper map: 37" x 37.5". Title: A physical inventory of streams in the Upper Willamette Watershed above the confluence of middle and coast forks of Willamette River : 1964 Author: Oregon. State Game Commission. Basin Investigations Section, Thompson, Kenneth E. Dimensions of paper map: 37" x 37.5". Close

• 38. [Article] FEMA floodplain geographic data for select streams in Wallowa County, Oregon

  This product is for informational purposes and may not have been prepared for, or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary ...

  Citation × Citation Citation Abstract Copy Title: FEMA floodplain geographic data for select streams in Wallowa County, Oregon Author: Smith, Dawn, Thomas, Samuel, Oregon State University This product is for informational purposes and may not have been prepared for, or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to verify the purpose and limitations. The data is provided as-is, without warranty. Title: FEMA floodplain geographic data for select streams in Wallowa County, Oregon Author: Smith, Dawn, Thomas, Samuel, Oregon State University This product is for informational purposes and may not have been prepared for, or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to verify the purpose and limitations. The data is provided as-is, without warranty. Close

• 39. [Article] Geospatial depiction of rivers and streams located within Wallowa County, Oregon

  This product is for informational purposes and may not have been prepared for, or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary ...

  Citation × Citation Citation Abstract Copy Title: Geospatial depiction of rivers and streams located within Wallowa County, Oregon Author: Northwest Hydrography Framework, Thomas, Samuel, Oregon State University This product is for informational purposes and may not have been prepared for, or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to verify the purpose and limitations. The data is provided as-is, without warranty. Title: Geospatial depiction of rivers and streams located within Wallowa County, Oregon Author: Northwest Hydrography Framework, Thomas, Samuel, Oregon State University This product is for informational purposes and may not have been prepared for, or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to verify the purpose and limitations. The data is provided as-is, without warranty. Close

• 40. [Article] Stream channel response to peak flows in a fifth-order mountain watershed

  This investigation explored how the magnitude, style, and frequency of channel adjustments vary spatially and over time within a 5th-order mountain watershed. Historical data sets, including repeated cross ...

  Citation × Citation Citation Abstract Copy Title: Stream channel response to peak flows in a fifth-order mountain watershed Author: Faustini, John M. This investigation explored how the magnitude, style, and frequency of channel adjustments vary spatially and over time within a 5th-order mountain watershed. Historical data sets, including repeated cross section surveys spanning up to 20 years at five sites on 2nd to 5th-order channels and streamflow records spanning up to 50 years, were supplemented by mapping and field reconnaissance activities. The study had two major parts. The first focused on two adjacent, contrasting stream reaches to examine the influence of large woody debris (LWD) on channel morphology and channel response to peak flows in a 3rd-order stream. The upper reach flows through old-growth forest with abundant LWD, while the lower reach was clearcut in 1964-65 and contains little LWD. A 25-year flood in 1996 caused deposition upstream of LWD steps in the old-growth reach alternating with scour between steps, resulting in no net gain or loss of sediment within the reach, while extensive scour and coarsening of the bed occurred in the clearcut reach. These observations suggest that reach-scale channel response was strongly influenced by LWD abundance, but that response at finer scales depends critically on the details of the location and arrangement of LWD. The second part of the study examined the dynamics of channel response to peak flows over two decades, and to two particular large floods during that period, in different portions of the channel network. The cross section data show that the streambed at the study sites is very stable, particularly in lower-order channels. Peak flows that produced detectable change at 90% of cross sections-flows able to cause significant channel adjustments-recur approximately three times as frequently (every 6-7 years) in 4`" to 5`h-order Lookout Creek as in 3rd-order Mack Creek (20-25 years). Flows that produced detectable change at 25% of cross sections are estimated to occur on average every 1.7 to 3.0 years at the study sites. It is estimated that if peak flows of all sizes were increased by only 10% due to anthropogenic impacts (e.g., logging) or climate change, the frequency of peak flows of a magnitude observed to produce significant channel adjustments would increase by approximately 30% in Lookout Creek and 60% in Mack Creek. Title: Stream channel response to peak flows in a fifth-order mountain watershed Author: Faustini, John M. This investigation explored how the magnitude, style, and frequency of channel adjustments vary spatially and over time within a 5th-order mountain watershed. Historical data sets, including repeated cross section surveys spanning up to 20 years at five sites on 2nd to 5th-order channels and streamflow records spanning up to 50 years, were supplemented by mapping and field reconnaissance activities. The study had two major parts. The first focused on two adjacent, contrasting stream reaches to examine the influence of large woody debris (LWD) on channel morphology and channel response to peak flows in a 3rd-order stream. The upper reach flows through old-growth forest with abundant LWD, while the lower reach was clearcut in 1964-65 and contains little LWD. A 25-year flood in 1996 caused deposition upstream of LWD steps in the old-growth reach alternating with scour between steps, resulting in no net gain or loss of sediment within the reach, while extensive scour and coarsening of the bed occurred in the clearcut reach. These observations suggest that reach-scale channel response was strongly influenced by LWD abundance, but that response at finer scales depends critically on the details of the location and arrangement of LWD. The second part of the study examined the dynamics of channel response to peak flows over two decades, and to two particular large floods during that period, in different portions of the channel network. The cross section data show that the streambed at the study sites is very stable, particularly in lower-order channels. Peak flows that produced detectable change at 90% of cross sections-flows able to cause significant channel adjustments-recur approximately three times as frequently (every 6-7 years) in 4`" to 5`h-order Lookout Creek as in 3rd-order Mack Creek (20-25 years). Flows that produced detectable change at 25% of cross sections are estimated to occur on average every 1.7 to 3.0 years at the study sites. It is estimated that if peak flows of all sizes were increased by only 10% due to anthropogenic impacts (e.g., logging) or climate change, the frequency of peak flows of a magnitude observed to produce significant channel adjustments would increase by approximately 30% in Lookout Creek and 60% in Mack Creek. Close